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| 1 | Progress and Prospects of Salt Lake Research in China显示文摘China has unique salt lake resources, and they are distributed in the east of Eurasian salt lake subzone of the Northern Hemisphere Salt Lake Zone, mainly concentrated in the regions with modern mean annual precipitation lower than 500 mm. This paper preliminarily reviews the progress made in salt lake research in China for the past 60 years. In the research of Paleoclimate and paleoenvironment from salt lake sediments, a series of salts have been proposed to be indicators of paleoclimate, and have been well accepted by scholars. The chloride-sulfate depositional regions of the west Qaidam and the east Tarim have been revealed to be the drought center of China since the Quaternary, and more than 6 spreading stages of arid climate(salt forming) have been identified. Five pan-lake periods with highstands have been proved to exist during the late Quaternary on the Tibetan Plateau. In mineral resource prospecting and theories of the forming of salt deposits: the atlas(1:2500000) of hydrochemical zoning of salt lakes on the Tibetan Plateau has been compiled for the first time, revealing the zonal distribution and transition from carbonate type to chloride type from south to north and presenting corresponding mineral assemblages for different type of salt lakes; several large continental salt deposits have been discovered and the theory of continental potash deposition has been developed, including the salt deposition in deep basins surrounded by high mountains, the mineral deposition from multistage evolution through chains of moderate or shallow lakes with multilevels, the origin of potassium rich brines in gravel layers, and the forming of potassium deposits through the inheriting from ancient salt deposits, thus establishing the framework of 'Continental Potash Deposition Theory'; several new types of Mg-borate deposits have been discovered, including the ulexite and pinnoite bed in Da Qaidam Lake, Qinghai, the pinnoite and kurnakovite bed in Chagcam Caka, Tibet, the kurnakovite bed in Lake Nyer, and the corresponding model of borate deposition from the cooling and dissolution of boron rich brines was proposed based on principles of geology, physics and chemistry. The anti-floatation-cold crystallization method developed independently has improved the capacity of KCl production to 3 million tons per year for the Qarham, serving the famous brand of potash fertilizer products. One 1.2 million ton K-sulfate production line, the biggest in the world, has been built in Lop Nor, and K-sulfate of about 1.6 million tons was produced in 2015. Supported by the new technology, i.e. brine preparation in winter-cooling-solarization-isolation-lithium deposition from salt gradient solar pond' the highest lithium production base at Zabuye Lake(4421 m), Tibet, has been established, which is the first lithium production base in China that reaches the year production of 5000 tons of lithium carbonate. The concept of Salt lake agriculture(Salt land agriculture) has been established based on the mass growth of Dunaliella and other bacillus-algae and the occurrence of various halophytes in saltmarsh and salt saline-alkali lands, finding a new way to increase arable lands and develop related green industry in salt rich environments. Finally this paper presents some new thoughts for the further research and development on salt science, and the further progress in salt science and technology will facilitate the maturing of the interdisciplinary science 'Salinology'. | ZHENG Mianping ZHANG Yongsheng LIU Xifang NIE Zhen KONG Fanjing QI Wen Jia Qingxian PU Linzhong HOU Xianhua WANG Hailei ZHANG Zhen KONG Weigang LIN Yongjie | 2016 | Acta Geologica Sinica(English Edition)2016，90，4： | 15 |
| 2 | A Comparative Analysis of Evaporate Sediments on Earth and Mars: Implications for the Climate Change on Mars显示文摘The knowledge of Martian salts has gone through substantial changes during the past decades. In the 70th of last century, Viking landers have noticed the existence of salts on Mars. Several salt species have been suggested from then on, such as sulfates and chlorides. However, their origin was a mystery due to the lack of observations. The recent explorations and related studies at the beginning of this century revealed that the crustal composition of Mars is similar to that of Earth, and it was hypothesized that almost one third of Martian surface was covered by oceans and lakes in the early stage of Mars. The huge water bodies may have dissolved a large quantity of ions from Martian primary rocks during the whole Noachian and Hesperian epoch. After the enormous drought event happened during the late Hesperian and the early Amazonian, these dissolved ions have formed huge salts deposits and most of them were preserved on Mars until today. To date, carbonates, sulfates, chlorides have all been detected by orbital remote sensing and by landers and rovers. However, the salt mineral assemblages on Mars seems to have some differences from those on Earth, e.g., rich in sulfates and lack of massive carbonates. To explain this difference, we propose that most of the surface carbonates precipitated from the ancient oceans may have been dissolved by the later ubiquitous acidic fluids originated from the global volcanism in the Hesperian era, and formed the enormous sulfate deposits as detected, and this hypothesis seems to be supported by the evidence that most of the sulfate deposits distribute around the Tharsis volcanic province while the survived carbonates located far from it. This process can release most of the carbon on Mars to the atmosphere in the form of CO2 and then be erased by the late heavy bombardments, which might have profound influence on the climate change happened in the Hesperian age. The positive correlation between the GRS results of the potassium distributions and the distribution of chlorides on Mars, together with the high Br concentration measured from the evaporate sediments at two Mars exploration rover landing sites, indicate that the brines in the regions where the chlorides deposited may have reached the stage for potassium salts deposition, thus we propose for the first time that potassium salts deposits might be prevalent in these regions. | ZHENG Mianping KONG Weigang ZHANG Xuefei CHEN Wenxi KONG Fanjing | 2013 | Acta Geologica Sinica(English Edition)2013，87，3： | 7 |
| 3 | Results of an Intentional Introduction of Artemia sinica in the High-Altitude Tibetan Lake Dangxiong Co:On a Base of Surveys in 2011 and 2013显示文摘1 Introduction The human population is projected to reach 9200million by 2050.A fundamental question for science is whether it is possible to increase food production to meet the demands of a human population of that magnitude.It’s possible only to increase an aquaculture production.Cultivation of fish/shrimp larvae is a bottleneck in a cultivation of the different organisms.Live | JIA Qinxian Elena ANUFRIIEVA LIU Shasha LIU Xifang KONG Fanjing ZHENG Mianping Nickolai SHADRIN | 2014 | Acta Geologica Sinica(English Edition)2014，88，S1： | 2 |
| 4 | Microbial Mats in Tibetan Hot Springs and their Contributions to the Cesium-bearing Geyserite Ore Formation显示文摘Microbial mats,mainly dominated by filamentous algae Calothrix and Oscillatoria,are well developed in Tibetan hot springs.A great number of fossil microorganisms,which existed as algae lamination in thermal depositional cesium-bearing geyserite in this area,are identified as Calothrix and Oscillatoria through microexamination and culture experiments.These microbial mats show the ability to accumulate cesium from spring water to the extent of cesium concentration of 0.46-1.03% cell dry weight,900 times higher than that in water,and capture large numbers of cesium-bearing opal grain.Silicon dioxide colloid in spring water replaces and fills with the organism and deposits on it to form algae laminated geyserite after dehydration and congelation.Cesium in the microbial mats and opal grain is then reserved in the geyserite.Eventually,cesium-bearing algae laminated geyserite is formed.Study on cesium distribution in geyserite also shows that cesium content in algae lamination,especially in heavily compacted algae lamination,is higher than in the opal layer.For geyserite with no algae lamination or other organism structure,which is generally formed in spring water with low silicon content,cesium accumulation and cesium-bearing opal grain assembled by the microbial mats are also indispensable.After the microbial mats accumulating cesium from spring water,silicon dioxide colloid poorly replaces and fills with the organism to form opal grain-bearing tremellose microbial mats.The shape and structure of the organisms are then destroyed,resulting in cesium-bearing geyserite with no algae lamination structure after dehydration and congelation.It is then concluded that microbial mats in the spring area contribute to the enrichment of cesium in the formation of cesium-bearing geyserite,and a biological genesis of the geyserite,besides of the physical and chemical genesis,is likely. | WANG Hailei ZHENG Mianping KONG Fanjing | 2012 | Acta Geologica Sinica(English Edition)2012，86，1： | 2 |
| 5 | Rapiddecolorizationofazodyemethylorangeinaqueoussolutionbynanoscalezerovalentironparticles显示文摘 | FanJing GuoYanhui WangJianji etal | 2009 | JournalofHazardousMaterials2009，166，23： | 1 |
| 6 | 显示文摘 | 梁旭华(LiangXH) 樊君(FanJ) 孙洋(SunY) 谭春雷(FanCL) | 2012 | 中国新药杂志2012，22，： | 1 |
| 7 | A general simulation model for performance prediction of plate fin-aM-tube heat exchanger with complex circuit configuration 显示文摘 | Ding W K FanJ F He Y L | 2011 | Applied Thermal Engineering2011，31，16： | 1 |
| 8 | Theinhibitionof18p-glycyrrhetinicacidonhumangastriccancercellBgc823prolifera-tion[J]显示文摘 | WANGYH FANJ ZHANGYL etal | 2007 | 江苏大学学报:医学版2007，17，3： | 1 |
| 9 | The benefits and costs of group affiliation: Evidence from East Asia显示文摘 | Claessens S FanJ P Lang L H | 2006 | Emerging Markets Review2006，7，1： | 1 |
| 10 | China's natural gas pricing reform may further delay under inflationary pressure'显示文摘 | Lin Fanjing | 2010 | China OGP2010，1，： | 1 |
| 11 | In vitro engineered cartilage using synovium-derived mesenchymal stem cells with injectable gellan hydrogels显示文摘 | FanJ Gong Y Ren L | 2010 | Acta Biomater2010，6，3： | 1 |
| 12 | Human tracking using convolutionalneural networks显示文摘 | FanJ Xu W Wu Y | 2010 | IEEE Transactions on Neural Networks2010，，10： | 1 |
| 13 | Synthesis of a novel cyclodextrin-derived chiral stationary phase with multiple urea linkages and enantioseparation toward chiral osmabenzene complex显示文摘 | Lin C Liu W N FanJ | 2013 | Journal of Chromatography A2013，1283，： | 1 |
| 14 | BiotemplatedpreparationofCdSnanoparticles/bacterialcellulosehybridnanofibersforphotocatalysisapplication显示文摘 | YangJ YuJ FanJ etal | 2011 | JournalofHazardousMaterials2011，189，1： | 1 |
| 15 | Epidemiology of non-alcoholicfatty liver disease in China显示文摘 | FanJ G Farrell GC | 2009 | J Hepatol2009，50，1： | 1 |
| 16 | Syntlle sis of thermosensitive poly (N-isopropylacrylamideco-acrylic acid)bydrogels with expanded network structures and improved oscillating swelling-deswelling properties显示文摘 | Zhang Xianzheng Yang Yiyan Wang Fanjing | 2002 | Langmuir2002，18，： | 1 |
| 17 | Idea of screening new aminoglycoside antibiotics and developing of etimicin [ J ]显示文摘 | ZhaoM FanJ | 2000 | 中国抗生素杂志2000，6，25： | 1 |
| 18 | 显示文摘 | 范杰(FanJ) 刘小闹(LiuXN) | | 化学通报0，，： | 1 |
| 19 | Semiparametric estimation of value at risk显示文摘 | FanJ GuJ | 2003 | EconometricsJournal2003，6，： | 1 |
| 20 | Institutions and organizational structure: the case of state-owned corpo- rate pyramids显示文摘 | FANJ P H WONG T J ZHANG T Y | 2013 | The Journal of Law Economics and Organization2013，29，6： | 1 |
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